Dastych, H. 2011. Bergtrollus Dzimbowski Gen. N., Sp. N., A

Total Page:16

File Type:pdf, Size:1020Kb

Dastych, H. 2011. Bergtrollus Dzimbowski Gen. N., Sp. N., A Entomol. Mitt. Zool. Mus. Hamburg 15 (186): 335-359 Hamburg, 1. Dezember 2011 ISSN 0044-5223 Bergtrollus dzimbowski gen. n., sp. n., a remarkable new tardigrade genus and species from the nival zone of the Lyngen Alps, Norway (Tardigrada: Milnesiidae) HIERONYMUS DASTYCH (with 51 gures) Abstract Bergtrollus dzimbowski gen. n., sp. n., a new genus and species of Tardigrada (the Milnesiidae) from moss in the nival zone of the Lyngen Alps (Norway), is described. This is the second milnesiid genus, apart from Milnesium Doyère, 1840, known to oc- cur in the Northern Hemisphere. The new tardigrade is characterized by a strikingly long and protrusible proboscis (‘snout’) formed by the prolonged mouth region. A simi- lar organ in Eutardigrada has also been reported in Milnesioides exsertum Claxton, 1999 and in the recently discovered Limmenius porcellus Horning et al., 1978 (see Claxton 1999) (both Milnesiidae). These species are known from limited records in New Zealand and Australia. The shape and length of the buccal tube in Bergtrollus gen. n. is intermediate between those of Milnesioides and Limmenius, but the mouth cavity is similar to Milnesium. Diagnostic morphological characters and identi cation key for all four genera of the Milnesiidae are presented and the phylogenetic status of the new taxon within the family is discussed. Keywords: Tardigrada, taxonomy, Bergtrollus dzimbowski gen. n., sp. n., nival zone, the Lyngen Alps, Norway, the Arctic. Introduction Milnesium tardigradum Doyère, 1840 is one of the rst described, still valid, worldwide recorded and commonly known tardigrades. The species repre- sents well-separated phyletic branch within Eutardigrada de ned by Schuster et al. (1980) as the order Apochela. The order consists of the sole fam- ily Milnesiidae Ramazzotti, 1962 with the three genera, Milnesium Doyère, 1840, Limmenius Horning et al., 1978 and Milnesioides Claxton, 1990. Within Milnesium more than 16 nominal species have been described in recent years (for a check-list see e.g., Guidetti & Bertolani 2005, Degma & Guidetti 2007). Two remaining genera are monospeci c and represented by Limmenius porcellus Horning, Schuster & Grigarick, 1978 and Milnesioides exsertum Claxton, 1999. These species, in particular L. porcellus, are char- acterized by a very long buccal tube, as compared to Milnesium. Moreover, 14674 - Entomologische Mitteilungen - Band 15 - Nummer 186.pdf 31 13.12.2011 09:05:32 336 DASTYCH, H. Figs 1-2. The type locality of Bergtrollus dzimbowski gen. n., sp. n.: general (1) and detailed (2) view. In the background E slope of the subsummit of Mt. Steindalstinden. 14674 - Entomologische Mitteilungen - Band 15 - Nummer 186.pdf 32 13.12.2011 09:05:32 Bergtrollus dzimbowski gen. n., sp. n. 337 the uppermost part of the head and mouth region in M. exsertum form a characteristic, extremely long ‘snout’ (Claxton 1999), a structure not known in other Eutardigrades. The presence of the snout (= proboscis) has also been discovered recently in the originally poorly described Limmenius (see Claxton, l.c.). While the members of Milnesium are common and distributed worldwide, those of Limmenius and Milnesioides have been recorded very rarely and only from the Southern Hemisphere. L. porcellus is known from a few localities in New Zealand (Horning et al. 1978) and from a single speci- men from Tasmania (Claxton 1999), while M. exsertum has been reported only from Australia, including Tasmania (Claxton, l.c.). When recently processing bryophytes from the Lyngen Alps (Northern Norway), several milnesiid tardigrades intermediate in their morphology be- tween Limmenius and Milnesioides were encountered. Analysis of the ma- terial brought to light a new and remarkable tardigrade genus and species and also the rst record of the second genus of the family Milnesiidae in the Northern Hemisphere. The paper describes the new tardigrade, compares it with other milnesiid genera and discusses its phylogenetic status within the family. Furthermore, a diagnostic key for these genera is provided. Material and Methods The new tardigrade were found in a small sample of moss (ca 7-10 cm2) collected in the nival zone of the Lyngen Alps, Norway (for details see “type locality” below). The moss was placed in a paper bag and air-dried. After seven months the sample was soaked in distilled water and kept overnight at the temperature of 0 °C. Tardigrades were extracted by the method described by Dastych (1985), with some living individu- als being observed under a stereo-microscope. The animals were [ xed for SEM ex- amination with hot Bouin’s medium, dehydrated, critical-point-dried and carbon-coated or, for light microscope study, killed with hot water and mounted in a Faure’s medium as permanent microslide preparations. One specimen (holotype) was xed in a mix- ture of methanol and acetic acid (3:1), stained with aceto-lactic orcein (see e.g. Berto- lani 1971) and mounted after examination, like other specimens, in Faure’s medium. Measurements were taken with PHC. The body length was measured without legs IV, mostly with retracted proboscis (‘snout’). The proboscis was fully extended in only two preserved individuals (one mounted for SEM: Figs 3, 11). However, as these ani- mals represent simplex-stage, their lamellar operculum and peribuccal papillae are torn away (Figs 15-17). Consequently, the proboscis was measured without these structures (slide no. 1982A, Table 1, column “b”: 80.1 m). The length of the organ, when available, was obtained indirectly from the remaining individuals (n = 3, holotype included), i.e. through adding lengths of retracted pseudosegments of the proboscis and that of lamellar operculum. The distance between the (upper) edge of the base of the cephalic papilla and the apex of the mouth region was considered as the length of the snout. The length of the bucco-pharyngeal and buccal apparatus includes peribuccal la- mellae. The term ‘buccal apparatus’ includes mouth cavity, buccal tube and associated structures; the ’bucco-pharyngeal apparatus’ embraces additionally the pharynx. The mouth cavity (= ‘mouth ring’ by Dewel & Clark 1973, in part) was measured with and 14674 - Entomologische Mitteilungen - Band 15 - Nummer 186.pdf 33 13.12.2011 09:05:33 338 DASTYCH, H. 14674 - Entomologische Mitteilungen - Band 15 - Nummer 186.pdf 34 13.12.2011 09:05:33 Bergtrollus dzimbowski gen. n., sp. n. 339 without the lamellae. The (external) diameter of the mouth cavity was taken at the bases of the peribuccal lamellae, immediately below their perpendicular striation. The mouth cavity length (that without lamellae) is the distance between the upper (strongly sclerotized) edge of the stylet sheaths and the level of the bases of peribuccal lamel- lae, just below their striation (comp. Claxton 1999). The length of the buccal tube was measured from the upper edge of the stylet sheaths up to the posterior edge of the tube, including terminal apophyses. The length of the buccal tube is made up of two units, i.e. that from the upper edge of the stylet sheaths up to the anterior edge of the stylet support insertion (= SSA unit; = pt ss index in Tumanov 2006, based on Pilato 1981) and that from the anterior (fore) edge of the stylet support insertion up to the posterior edge of the tube, including its terminal apophyses (= SSB unit). The (external) diameter of the tube is taken just above the insertion of the stylet supports. Two specimens (slide no. T1985c and T1982d) had on the left and right side of the tube different (aberrant) length of the unit SSB. The unit sides measured 58.3 vs. 63.0 and 61.1 vs. 64.8 m, respectively. Arbitrarily, the higher values of these lengths have been considered for calculations. The whole length of the primary (= main) branch of the claw was measured from the apex of accessory spines up to the external edge of the arch-like cuticular bar (mbb: Figs 30, 31), which bar is located dorsally and laterally at the nger-like base of the branch. The length of sclerotized unit of the primary branch was measured from the apex of accessory spines up to very proximal termination of its sclerotized com- ponent (= “main branch length” in Tumanov 2006: Fig. 1). The length (height) of the remaining (i.e. basal) part of claw (= ‘basal claw’: Fig. 29: bc) includes lunula (= ‘basal thickening’: e.g. Tumanov 2006) and is the distance between the tip of the secondary branch and the posterior edge of the lunula. An additional measurement of the basal claw excludes the lunula. The width of lunula is a diameter of the structure. The morphometric indices applied are de ned in Dastych (2006, 2011). For calcu- lation of the hind claw base index (“HBI”) only the sclerotized part of the claw main branch was considered [the length (height) of hind basal claw, lunula excluded x 100 / sclerotized unit of the hind claw main branch]. Furthermore, the following new mor- phometric indices have been introduced: 1) the snout / body index (“SBI”) i.e., the (percent) ratio between the length of the snout (proboscis) and the body; 2) the mouth cavity index (“MCAVI”) which describes the shape of the mouth cav- ity [the length of mouth cavity, peribuccal lamellae excluded x 100 / mouth cavity width]; 3) the hind claw lunula index (“HLI”) which de ned the size of the hind lunula (the hind claw lunula width x 100 / the basal claw length, lunula included). Microphotographs were taken with ZEISS ‘Fotomikroskop III’, SEM micrographs with LEO 1525. Figures 19, 23, 24, 34 come from the holotype of the new taxon, the other images represent paratypes. Figs 3-6. Bergtrollus dzimbowski gen. n., sp. n., animal in simplex-stage. 3. habitus: latero-dorsally, 4-6: apex of the proboscis (‘snout’) in latero-dorsal, latero-ventral and lateral view, respectively (peribucal lamellae and papillae torn out).
Recommended publications
  • Troms Og Finnmark
    Kommunestyre- og fylkestingsvalget 2019 Valglister med kandidater Fylkestingsvalget 2019 i Troms og Finnmark Valglistens navn: Partiet De Kristne Status: Godkjent av valgstyret Kandidatnr. Navn Fødselsår Bosted Stilling 1 Svein Svendsen 1993 Alta 2 Karl Tobias Hansen 1992 Tromsø 3 Torleif Selseng 1956 Balsfjord 4 Dag Erik Larssen 1953 Skånland 5 Papy Zefaniya 1986 Sør-Varanger 6 Aud Oddrun Grønning 1940 Tromsø 7 Annbjørg Watnedal 1939 Tromsø 8 Arlene Marie Hansen 1949 Balsfjord 04.06.2019 12:53:00 Lister og kandidater Side 1 Kommunestyre- og fylkestingsvalget 2019 Valglister med kandidater Fylkestingsvalget 2019 i Troms og Finnmark Valglistens navn: Høyre Status: Godkjent av valgstyret Kandidatnr. Navn Fødselsår Bosted Stilling 1 Christine Bertheussen Killie 1979 Tjeldsund 2 Jo Inge Hesjevik 1969 Porsanger 3 Benjamin Nordberg Furuly 1996 Bardu 4 Tove Alstadsæter 1967 Sør-Varanger 5 Line Fusdahl 1957 Tromsø 6 Geir-Inge Sivertsen 1965 Senja 7 Kristen Albert Ellingsen 1961 Alta 8 Cecilie Mathisen 1994 Tromsø 9 Lise Svenning 1963 Vadsø 10 Håkon Rønning Vahl 1972 Harstad 11 Steinar Halvorsen 1970 Loppa 12 Tor Arne Johansen Morskogen 1979 Tromsø 13 Gro Marie Johannessen Nilssen 1963 Hasvik 14 Vetle Langedahl 1996 Tromsø 15 Erling Espeland 1976 Alta 16 Kjersti Karijord Smørvik 1966 Harstad 17 Sharon Fjellvang 1999 Nordkapp 18 Nils Ante Oskal Eira 1975 Lavangen 19 Johnny Aikio 1967 Vadsø 20 Remi Iversen 1985 Tromsø 21 Lisbeth Eriksen 1959 Balsfjord 22 Jan Ivvar Juuso Smuk 1987 Nesseby 23 Terje Olsen 1951 Nordreisa 24 Geir-Johnny Varvik 1958 Storfjord 25 Ellen Kristina Saba 1975 Tana 26 Tonje Nilsen 1998 Storfjord 27 Sebastian Hansen Henriksen 1997 Tromsø 28 Ståle Sæther 1973 Loppa 29 Beate Seljenes 1978 Senja 30 Joakim Breivik 1992 Tromsø 31 Jonas Sørum Nymo 1989 Porsanger 32 Ole Even Andreassen 1997 Harstad 04.06.2019 12:53:00 Lister og kandidater Side 2 Kommunestyre- og fylkestingsvalget 2019 Valglister med kandidater Fylkestingsvalget 2019 i Troms og Finnmark Valglistens navn: Høyre Status: Godkjent av valgstyret Kandidatnr.
    [Show full text]
  • Kåfjord, Lyngen Og Storfjord
    Kåfjord, Lyngen og Storfjord Utredning av Lyngenfjordmodellen 15. oktober 2015 Lyngen kommune Strandveien 24 9060 Lyngseidet 15. oktober 2015 Lyngenfjordmodellen – et naturlig valg med felles kultur og historie Kommunene Kåfjord, Lyngen og Storfjord har tatt initiativ til en felles utredning av sammenslåing i den såkalte «Lyngenfjordmodellen» Utredningen skal være en del av beslutningsgrunnlaget når kommunene skal ta beslutning om ny kommunestruktur. Rapporten danner også grunnlag for eventuelt videre prosess fram mot en intensjonsavtale om kommunesammenslåing. PwC er hovedansvarlig for rapporten som er utarbeidet i samarbeid med våre underleverandører Stiftelsen Telemarksforsking og Burson-Marsteller AS. Oppdraget har blitt utført av et team bestående av Geir Are Nyeng, (prosjektleder), Wenche Vennes, Rolf Tørring, Geir Årset og Trond Solbakken fra PwC, Kjetil Lie og Audun Thorstensen fra Telemarksforsking, samt Peter Gitmark, Lars Vidar Gullestad og Erik Strøm fra Burson- Marsteller AS. Reinholdt Bredrup i PwC har vært ansvarlig partner på oppdraget. Fra oppdragsgivers side har prosjektet vært ledet av en arbeidsgruppe bestående Viggo Jørn Dale (prosjektleder) i Lyngen kommune, May-Tove Lilleng i Storfjord kommune og Håkon Jørgensen i Kåfjord kommune. Vi vil benytte anledningen til å takke for et godt samarbeid i forbindelse med utredningen. Vi vil også takke ansatte og folkevalgte i kommunene som har deltatt i intervjuer, svart på kommunenes egenvurdering og bidratt med annen informasjon. Dette har vært til stor nytte i utredningsarbeidet. Med vennlig hilsen Reinholdt Bredrup Geir Are Nyeng Partner Prosjektleder © 2014 PwC. Med enerett. I denne sammenheng refererer "PwC" seg til PricewaterhouseCoopers AS, Advokatfirmaet PricewaterhouseCoopers AS, PricewaterhouseCoopers Accounting AS, PricewaterhouseCoopers Skatterådgivere AS og PricewaterhouseCoopers Services AS som alle er separate juridiske enheter og uavhengige medlemsfirmaer i PricewaterhouseCoopers International Limited.
    [Show full text]
  • Toppturer Ski Touring
    NYHET! ALLE TURENE 1 KLASSIFISERT MED KAST TOPPTURER 2 NEW! ROUTES AT ALL SKI TOURING DIFFICULTY LEVELS 3 UTVALGTE SKITURER I SKJERVØY, KVÆNANGEN OG NORDREISA 25 SELECTED SKI TOURS IN NORDREISA, KVÆNANGEN AND SKJERVØY Foto/photo: Veri Media Veri Foto/photo: SKIOPPLEVELSER I VERDENSKLASSE WORLD CLASS SKIING ABOVE THE ARCTIC CIRCLE Foto/photo: Veri Media Veri Foto/photo: NATURALLY EXCITING LYNGENFJORD LYNGENFJORD LYNGENFJORD LYNGENFJORD FORORD Toppturer på ski er blitt en meget populær aktivitet. Over hele verden der skisport har fotfeste har interessen for såkalt «backcountry ski touring», eller toppturer som er det mest brukte norske ordet, økt de siste årene. Brosjyren er produsert av Fri Flyt og trykket på FSC sertifi- sert/resirkulert papir. Norge har også hatt stor økning i antall personer lingen som et bakteppe har vi nå gjennom prosjektet Grafisk utforming er gjort av som søker mot toppene med ski på beina. I nord «Bærekraftig utvikling av toppturdestinasjon Skjer- Mathilde Sjulstad. og kanskje i hele landet har Lyngsapene siden 1995 vøy, Kvænangen og Nordreisa» kartlagt regionens Prosjektet er eid av Visit vært det store lokomotivet i å trekke til seg topp- potensiale som toppturområde. Regionen innehar Lyngenfjord AS med Espen turturister. Da seilte den italiensk skiguiden Luca i utgangspunktet absolutt mange av de naturgitte Nordahl som prosjektleder. Kartene er laget av Mester- Casparini inn i området og viste oss den geniale kvaliteter som de allerede populære toppturområder kart med kartgrunnlag fra kombinasjonen for Kyst-Norge av å bo om bord i har med mye spennende fjellnatur og storslagen Statens Kartverk. KAST-klas- båt for å farte rundt til nye toppturmål hver dag.
    [Show full text]
  • Norwegian Eat Your Way Through Any Holiday with This Cookbook American Story on Page 12-13 Volume 127, #30 • November 4, 2016 Est
    the Inside this issue: NORWEGIAN Eat your way through any holiday with this cookbook american story on page 12-13 Volume 127, #30 • November 4, 2016 Est. May 17, 1889 • Formerly Norwegian American Weekly, Western Viking & Nordisk Tidende $3 USD Discovering Helgeland It’s never too late to uncover a new favorite part of Norway PATRICIA BARRY Hopewell Junction, N.Y. “What is your favorite place in Norway?” I world-famous Lofoten Islands, Helgeland— was asked during our trip there in June. Norway’s hidden gem—quietly displays its own I hesitated. Our family has covered lots of unique beauty. territory in Norway. We’ve been to every fylke Helgeland’s partially submerged lowlands (county) and seen more of Norway than most form thousands of skerries that dot the coast- Norwegians, we’ve been told. How could I pick line. Sharp, angular mountains (3,500 ft.) pop WHAT’S INSIDE? one favorite place? up along the coast. Add to this the white sandy And would my answer change? Every trip beaches, glaciers, fjords, inland forests and Nyheter / News 2-3 Du må tørre å ta modige to Norway we seek out new places. On this trip mountains, and the Arctic Circle and you have a « Business og krevende valg. Det finnes 4-5 Helgeland would be our new adventure. combination of features that makes Helgeland a Our entourage included my husband, our unique and stunning part of Norway. ikke noen snarvei. » Opinion 6-7 Sports 8-9 son, our former exchange student, her husband Easily accessible but not as crowded as – Celina Midelfart (our personal tour guide born and raised in Helge- more popular destinations, Helgeland beckons.
    [Show full text]
  • Tardigrades Colonise Antarctica?
    This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Short, Katherine A Title: Life in the extreme when did tardigrades colonise Antarctica? General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. A copy of this may be found at https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode This license sets out your rights and the restrictions that apply to your access to the thesis so it is important you read this before proceeding. Take down policy Some pages of this thesis may have been removed for copyright restrictions prior to having it been deposited in Explore Bristol Research. However, if you have discovered material within the thesis that you consider to be unlawful e.g. breaches of copyright (either yours or that of a third party) or any other law, including but not limited to those relating to patent, trademark, confidentiality, data protection, obscenity, defamation, libel, then please contact [email protected] and include the following information in your message: •Your contact details •Bibliographic details for the item, including a URL •An outline nature of the complaint Your claim will be investigated and, where appropriate, the item in question will be removed from public view as soon as possible. 1 Life in the Extreme: when did 2 Tardigrades Colonise Antarctica? 3 4 5 6 7 8 9 Katherine Short 10 11 12 13 14 15 A dissertation submitted to the University of Bristol in accordance with the 16 requirements for award of the degree of Geology in the Faculty of Earth 17 Sciences, September 2020.
    [Show full text]
  • 5 Northern Lights: Unparalleled Adventureland Access
    5 Northern Lights: Unparalleled NORTHERN LIGHTS AIRPORTS SVALBARD AIRPORT Main airport serving the Arctic archipelago of Svalbard. ALTA AIRPORT Adventureland access Flights to Oslo and Tromsø. The northernmost airport in The airport serves the municipality of Alta and the the world with publicly scheduled flights. Finnmark region. Daily flights to Oslo and regional FLIGHT MOVEMENTS: 3,000 / TOTAL PASSENGERS: 182,000 destinations. Has some international charter services. FLIGHT MOVEMENTS: 6,500 / TOTAL PASSENGERS: 387,000 TROMSØ AIRPORT The fifth-busiest airport in Norway and main hub for regional flights to the Finnmark region. There are B737 Services to Oslo and other major airports in Norway. International flights to several European destinations, as well as charter and seasonal services. HARSTAD/NARVIK AIRPORT FLIGHT MOVEMENTS: 36,000 / TOTAL PASSENGERS: 2,340,000 Harstad/Narvik Airport has one of Norway’s longest runways and is approved for use by Boeing 747 aircraft. FLIGHT MOVEMENTS: 10,000 / TOTAL PASSENGERS: 763,000 BODØ AIRPORT In addition to jet operations to major domestic destinations, Bodø airport serves Famous shark puncher and three-time world champion surfer as a hub for regional flights to Helgeland, Lofoten and Vesterålen. The airport has Mick Fanning rides the Northern Lights at Unstad beach in international routes and more than ten daily return flights to Avinor Oslo Airport. Lofoten. The technically challenging picture was shot by FLIGHT MOVEMENTS: 36 ,000 / TOTAL PASSENGERS: 1,825,000 Norwegian photographers Emil Sollie and Mats Grimsæth. PHOTO: EMIL SOLLIE, MATS GRIMSÆTH & RED BULL CONTENT POOL Northern Norway offers the world’s Five airports in Northern Norway offer excellent access to the • UNESCO World Heritage Rock Art Centre, Alta SEASONALITY 2018 600' best access to the Northern Lights Northern Lights: Bodø Airport, Harstad/Narvik Airport, Tromsø Airport, • Hurtigruten Norwegian coastal steamer tours Alta Airport and Svalbard Airport.
    [Show full text]
  • Download Itinerary
    NORTH NORWAY AND AURORA BOREALIS TRIP CODE ACOWNNJ DEPARTURE 02/01/2021, 09/02/2021, 16/01/2021, 23/01/2021, 30/01/2021, 20/11/2021, 27/11/2021. DURATION INTRODUCTION 8 Days Cruise along the serene and isolated fjords of Troms on this incredible 8 day voyage. On LOCATIONS board the Nooderlicht you will have a true expedition experience as you immerse yourself in the beauty of the Norwegian Fjords. Encounter more than one species of whale as well Norway as other unique wildlife including White-tailed eagles. The quaint Nooderlicht offers a smaller voyage capacity offering an intimate, flexible and completely immersive experience as you look out for the legendary Northern Lights. ITINERARY DAY 1: Embarkation in Tromoso Your adventure begins in Tromso, nicknamed the “Paris of the North,” located in an area rich with Norse and Sámi history. Enjoy exploring this sub Arctic Norwegian town, said to have been inhabited since the last ice age. All voyages with s/v Rembrandt van Rijn aim at departing from Tromsø in the evening of day one, while s/v Noorderlicht will set sail in the early morning of day two. All passengers of Rembrandt are kindly asked to board the vessel by 17:00, while passengers of Noorderlicht are welcome to board the vessel between 17:00 and 23:00. Copyright Chimu Adventures. All rights reserved 2020. Chimu Adventures PTY LTD NORTH NORWAY AND AURORA BOREALIS DAY 2: Into The Nordic Fjords - Day 2 to 6 TRIP CODE You then sail along the base of the Lyngen Alps, across the Lyngen fjord, and may stay for the ACOWNNJ night in Hamnnes, on the island of Uloya.
    [Show full text]
  • Tardigrades of the Tree Canopy: Milnesium Swansoni Sp. Nov. (Eutardigrada: Apochela: Milnesiidae) a New Species from Kansas, U.S.A
    Zootaxa 4072 (5): 559–568 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2016 Magnolia Press ISSN 1175-5334 (online edition) http://doi.org/10.11646/zootaxa.4072.5.3 http://zoobank.org/urn:lsid:zoobank.org:pub:8BE2C177-D0F2-41DE-BBD7-F2755BE8A0EF Tardigrades of the Tree Canopy: Milnesium swansoni sp. nov. (Eutardigrada: Apochela: Milnesiidae) a new species from Kansas, U.S.A. ALEXANDER YOUNG1,5, BENJAMIN CHAPPELL2, WILLIAM MILLER3 & MARGARET LOWMAN4 1Department of Biology, Lewis & Clark College, Portland, OR 97202, USA. 2Department of Biology, University of Kansas, Lawrence, KS 66045, USA. 3Department of Biology, Baker University, Baldwin City, KS 66006, USA. 4California Academy of Sciences, San Francisco, California 94118, USA. 5Corresponding author. E-mail: [email protected] Abstract Milnesium swansoni sp. nov. is a new species of Eutardigrada described from the tree canopy in eastern Kansas, USA. This species within the order Apochela, family Milnesiidae, genus Milnesium is distinguished by its smooth cuticle, nar- row buccal tube, four peribuccal lamellae, primary claws without accessory points, and a secondary claw configuration of [3-3]-[3-3]. The buccal tube appears to be only half the width of the nominal species Milnesium tardigradum for animals of similar body length. The species adds to the available data for the phylum, and raises questions concerning species dis- tribution. Key words: Four peribuccal lamellae, Thorpe morphometry, Tardigrada, Canopy diversity Introduction Milnesium Doyère, 1840 is a genus of predatory limno-terrestrial tardigrades within the Order Apochela and the Family Milnesiidae with unique morphological characteristics (Guil 2008). The genus is distinct within the phylum Tardigrada for lacking placoids, but having peribuccal papillae, lateral papillae, peribuccal lamellae, a wide buccal tube, and separated double claws (Kinchin 1994).
    [Show full text]
  • Gaivouna / Kåfjord, Lyngen Og Storfjord Kommune
    PLANBESKRIVELSE 17.10. 2013 Interkommunal kystsoneplan for: Gaivouna / Kåfjord, Lyngen og Storfjord kommune SISTE REVISJON: 24.06.14 1 INNHOLD BAKGRUNN Et interkommunalt samarbeidsprosjekt 05 1 INNLEDNING 06 1.1 Lokalisering 06 1.2 Plantype 06 1.3 Plandokumenter 06 1.4 Planens formål 07 1.5 Effektmål 07 1.6 Rettsvirkning 07 1.7 Overordnede rammer og føringer 08 1.8 Interkommunalt plansamarbeid 08 1.9 Organisering av planarbeidet 09 1.10 Planprosess 09 1.11 Veien videre 10 1.12 Planens avgrensning 10 1.13 Geografisk avgrensning 10 2 INNSPILL TIL PLANEN 11 2.1 Plandokumenter 11 2.2 Politiske innspill til planen for eventuell oppfølging 12 3 BESKRIVELSE AV PLANTEMA 14 3.1 Lyngenfjorden 14 3.2 Nøkkeltall 14 3.3 Bebyggelse 14 3.4 Strandsonen 14 3.5 Landbruk 15 3.6 Reindrift 15 3.7 Forsvaret 16 3.8 Friluftsliv 16 3.9 Båndlagte områder 17 3.10 Biologisk mangfold 17 3.11 Tradisjonell bruk, samisk kultur, utmarksnæring og samfunnsliv 19 3.12 Småbåthavn 19 3.13 Ferdsel/farleder 19 3.14 Fiskeri 19 3.15 Akvakultur 21 3.16 Sikringssoner anadrom fisk 22 3.17 Samfunnssikkerhet 22 4 HOVEDTREKK I PLANARBEIDET 25 4.1 Strategiske valg 26 4.2 Om kartdelen 26 4.3 Om arealformål 26 5 BESKRIVELSE AV DE ENKELTE AREALFORMÅL 27 5.1 Bebyggelse og anlegg 27 5.2 Samferdselsanlegg og teknisk infrastruktur 27 5.3 Grønnstruktur 27 5.4 Forsvaret 27 5.5 Landbruks- natur- og friluftsområder, samt reindrift 28 5.6 Bruk og vern av sjø og vassddrag med tilhørende strandsone 28 5.6.1 Flerbruksområder 28 5.6.2 Ferdsel 29 5.6.3 Småbåthavn 29 5.6.4 Fiskeri 29 5.6.5 Akvakultur 30 5.6.6 Kombinerte formål 30 5.6.7 Naturområder 31 5.6.8 Friluftsområder i sjø.
    [Show full text]
  • Tectonostratigraphic Succession and Development of the Finnmarkian Nappe Sequence, North Norway K
    Tectonostratigraphic Succession and Development of the Finnmarkian Nappe Sequence, North Norway K. B. ZWAAN & D. ROBERTS Zwaan, K. B. & Roberts, D. 1978: Tectonostratigraphic succession and devel opment of the Finnmarkian nappe sequence, North Norway. Norges geol. Unders. 343, 53-71. Detailed investigations of the Finnmarkian nappe sequence within the 1:250 000 map-sheets 'Hammerfest', 'Nordreisa' and 'Honningsvåg' have revealed a complex construction of discrete nappes, sub-nappes and minor thrust slices. In the Kalak (Reisa) Nappe Complex the nappes are composed not only of the übiquitous Vendian to Cambrian lithostratigraphy but also of proven (dated) or suspected, older, Precambrian, high-grade gneissic/amphibolitic units and slices of Raipas carbonates and volcanites. In places, thick sequences of gneisses and schists have been converted to blastomylonites and locally ultramylonites, mainly during the first two of four principal deformation episodes. On a regional scale, major Dj folds are present in northwesterly areas whereas further southeast a more homogeneous flattening deformation prevailed. D 2 fold structures, related to the regionally developed principal foliation, show a variable development in style and trend with fold axial rotations into a NW-SE trend related to high internal strains, noticeably towards the lower parts of the nappe units. These deformations were wholly Finnmarkian (late Cambrian - early Ordovician). Nappe translation, linked to D 2, diminished in magnitude towards the northeast. Later deformation episodes include imbrication structures on all scales which can be shown to relate to the thrusting of higher nappes containing Ordo-Silurian stratigraphies. These date to late Silurian time. The Silurian emplaced nappes continue southwards into the well-documented nappe complexes of Nordland and Trøndelag.
    [Show full text]
  • Status for Interkommunalt Samarbeid I Troms Og Finnmark
    NIVI Rapport 2019:4 Status for interkommunalt samarbeid i Troms og Finnmark Utarbeidet på oppdrag av Fylkesmannen Notat 2020- Av Geir Vinsand - NIVI Analyse AS FORORD På oppdrag fra Fylkesmannen i Troms og Finnmark har NIVI Analyse gjennomført en kartlegging av det formaliserte interkommunale samarbeidet i alle fylkets 43 kommuner. Kartleggingen har form av en kommunevis totalkartlegging og bygger på NIVIs kartleggingsmetodikk som er brukt i flere andre fylker. Prosjektet er gjennomført i nær dialog med Fylkesmannen og rådmennene i kommunene. Prosjektet ble startet opp i august 2019. Kontaktperson hos oppdragsgiver har vært fagdirektør Jan-Peder Andreassen. NIVI er ansvarlig for alle analyser av innsamlet materiale, inkludert løpende problematiseringer og anbefalinger. Ansvarlig konsulent i NIVI Analyse har vært Geir Vinsand. Sandefjord, 20. desember 2019 1 - NIVI Analyse AS INNHOLD HOVEDPUNKTER ................................................................................................. 3 1 METODISK TILNÆRMING ........................................................................ 6 1.1 Bakgrunn og formål ............................................................................. 6 1.2 Problemstillinger .................................................................................. 6 1.3 Definisjon av interkommunalt samarbeid ............................................ 7 1.4 Gjennomføring og erfaringer ............................................................... 8 1.5 Rapportering .......................................................................................
    [Show full text]
  • A Checklist of Norwegian Tardigrada
    Fauna norvegica 2017 Vol. 37: 25-42. A checklist of Norwegian Tardigrada Terje Meier1 Meier T. 2017. A checklist of Norwegian Tardigrada. Fauna norvegica 37: 25-42. Animals of the phylum Tardigrada are microscopical metazoans that seldom exceed 1 mm in length. They are recorded from terrestrial, limnic and marine habitats and they have a distribution from Arctic to Antarctica. Tardigrades are also named ‘water bears’ referring to their ‘walk’ that resembles a bear’s gait. Knowledge of Norwegian tardigrades is fragmented and distributed across numerous sources. Here this information is gathered and validity of some records is discussed. In total 146 different species are recorded from the Norwegian mainland and Svalbard. Among these, 121 species and subspecies are recorded in previous publications and another 25 species are recorded from Norway for the first time. doi: 10.5324/fn.v37i0.2269. Received: 2017-05-22. Accepted: 2017-12-06. Published online: 2017-12.20. ISSN: 1891-5396 (electronic). Keywords: Tardigrada, Norway, Svalbard, checklist, taxonomy, literature, biodiversity, new records 1. Prinsdalsfaret 20, NO-1262 Oslo, Norway. Corresponding author: Terje Meier E-mail: [email protected] INTRODUCTION terminating in claws or sucking disks. The first three pairs of legs are directed ventrolaterally and are used to moving over the The phylum Tardigrada (water bears) currently holds about substrate. The hind legs are directed posteriorly and are used for 1250 valid species and subspecies (Degma et al. 2007, Degma grasping. Adult Tardigrades usually range from 250 µm to 700 et al. 2017) and are found in a great variety of habitats. They µm in length.
    [Show full text]